publications > paper > surface-water transport of suspended matter through wetland vegetation of the Florida everglades > experimental methodology
Surface-water transport of suspended matter through wetland vegetation of the Florida everglades
3. Experimental Methodology[5] Particles composed of titanium dioxide (TiO2) with an average diameter of 0.3 µm were suspended in filtered (0.2 µm) Everglades water and used as the tracer. Background concentrations of TiO2 in Shark River Slough are low, so the TiO2 tracer particles could be distinguished from the autochthonous particles on the basis of their chemical signature.[6] We introduced a 9 g/L TiO2 suspension 0.7 m upgradient of the leading edge of the vegetation, which was located approximately 10 m from the head of the channel (Figure 1a). The injection was accomplished by using a metering pump to deliver the TiO2 tracer at constant rate (100 mL/min) through a slotted hose that spanned the central 1.8 m of the channel and rested 24 cm below the water surface (Figure 1b). The duration of the injection was 0.9 hours. Sampling for the TiO2 began before the start of the injection and continued for 3 hours after its termination. Water samples (20 mL) were repeatedly collected in plastic scintillation vials by applying suction to 1/8" stainless steel sampling tubes installed at discrete points located 6.8 m down channel from the injection (Figures 1a and 1b). The sampling points were designated as LS, LM, LD, CM, RS, RM, and RD, where L (left), C (center), and R (right) delineate lateral position and refer to locations 0.8 m inside the left wall, at the channel center, and 0.8 m inside the right wall, respectively, and S (shallow), M (mid-depth), and D (deep) delineate vertical position and refer to depths of 0.15, 0.27, and 0.42 m, respectively. Concentrations of titanium (Ti) in the surface-water samples were measured in the laboratory by inductively coupled plasma mass spectrometry following acid dissolution of the TiO2 particles.
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U.S. Department of the Interior, U.S. Geological Survey
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